GB2154998A

GB2154998A - Randomly interstratified clays

Info

Publication number: GB2154998A
Application number: GB08505332A
Authority: GB
Inventors: Paul Henry Nadeau
Original assignee: National Research Development Corp UK
Current assignee: National Research Development Corp UK
Priority date: 1984-03-02
Filing date: 1985-03-01
Publication date: 1985-09-18
Also published as: EP0153879B1; MX164876B; JPH06100315A; JPH0678163B2; CA1242685A; ATE58514T1; AU3879985A; AU577736B2; JPS60210516A; GB8505332D0; US4687521A; GB8405531D0; GB2154998B; JPH0621028B2; EP0153879A3; EP0153879A2; DE3580600D1

Abstract

Randomly interstratified clay is synthesised by:(i) saturating (replacing all the exchangeable cations of) a first clay with alkali metal ions (preferably Na- or Li+), removing any excess alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 10-7m equivalent spherical diameter,(ii) saturating a second clay with alkali metal ions (preferably Na+ or Li-), removing any excess alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 10-7m equivalent spherical diameter,(iii) mixing the suspensions from (i) and (ii) to form a mixed suspension, and(iv) sedimenting and optionally drying the mixed suspension, the sediment being the synthetic randomly interstratified clay.A wider range of synthetic clay compositions is thereby made available for use as catalysts, sorbents etc.

Description

(12) UK Patent Application (,,)GB (1,) 2 154 998 A (43) Application

published 18 Sep 1985 (21) Application No 8505332 (5 1) INT CL 4 C01 B 33/20 (22) Date of filing 1 Mar 1985 (30) Priority data (31) 8405531 (32) 2 Mar 1984 (33) GB (52) Domestic classification CIA 421 425 M 10 M5 M7 M9 PS U1S 1345 1356 C1A (56) Documents cited GB 1593382 GB 1571983 GB 1467601 GB 0949436 GB 1052983 GB 0845645 (71) Applicant National Research Development Corporation (United Kingdom), 101 Newington Causeway, London SE1 6BU (58) Field of search CIA (72) Inventor Paul Henry Nadeau (74) Agent and/or Address for Service P W Neville, Patent Department, National Research Development Corporation, 101 Newington Causeway, London SE1 6BU ERRATUM

SPECIFICATION NO 2154998A

Page NO 3 Line NO 31 after smectite: for rectorite read corrensite Page No 3 Line NO 35 for 1-1 read 1:1 THE PATENT OFFICE 4 March 1986 G) C0 l\i (71 -P-,, (D (D 00 1 GB 2 154 998A 1 SPECIFICATION

Randomly interstratified clays This invention relates to randomly interstratified clays, to a method of synthesising randomly 5 interstratified clays, and to an intermediate in the method.

Clays have a layer silicate structure. In a pure clay, the layers are all the same. If two or more different kinds of layer(s) occur within a sequence of layers, the clay is described as interstratified. If the sequence of the different layers is regular, for example as in certain naturally occurring deposits of K-rectorite (an interstratification of illite and smectite), the clay is 10 known as regularly interstratified. If the sequence is random, the clay is randomly interstratified.

Interstratified clays in nature almost always contain expandable layers, usyally classified as smectite or vermiculite. Such layers are capable of adsorbing exchangeable cations, water and/or organic molecules. Smectite is a general term, examples of which include montmorillon ite, beidellite, nontronite, saponite and hectorite. 1 Clays are widely used in industry, for example as catalysts, catalytic supports, chemical supports, coagulants, sorbents and colloidal stabilisers. Generally, in industry, the best clay (or clay mixture) for a given purpose is determined not by systematic evalutions of every possible composition, but by selecting on a trial-and-error basis from whatever natural deposits happen to be available. This practice has persisted because of the difficulty or cost of hydrothermally or 20 otherwise synthesising clays of compositions chosen at will. Simply mixing suspensions of two different clays has led to products which are merely segregated physical mixtures of the two starting clays.

According to the present invention, a randomly interstratified clay is synthesised by:- (i) saturating (replacing all the exchangeable cations of) a first clay which is either fully 25 expandable or contains an expandable component, with alkali metal ions (preferably Nal or Li+), removing any excess alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 10-7m equivalent spherical diameter, (ii) separately or together saturating a second clay which is either fully expandable or contains an expandable component, with alkali metal ions (preferably Na+ or Li+), removing any excess 30 alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 10-7M spherical diameter, (iii) forming a mixed suspension from the suspension from (i) and (ii), and (iv) sedimenting and optionally drying the mixed suspension, the sediment being the synthetic randomly interstratified clay.

"Equivalent spherical diameter- refers to Stokes' Law about spherical bodies failing in fluids; the relative density of the particles is assumed to be 2.5.

The steps (i) and (ii) may be performed together in the same vessel in which case the mixing step (iii) is normally inherent and simultaneous; otherwise an actual mixing must be performed.

After sedimenting and/or optional drying, the product may be saturated with any desirable 40 cation.

The expandable component will in general always be a smectite or a vermiculite.

This synthetic randomly interstratified clay will have in general the composition represented by the suspension (i) and (ii) in their starting proportions. Some such compositions of synthetic clays will also be found in nature, but most will be entirely new. Furthermore suspension(s) (ii).... may be added (under corresponding conditions) to make three or more-component randomly interstratified clays, all of which except illite-chlorite-smectite and illite- smectitevermiculite (we believe) are new products, not found in nature at all.

The invention extends to randomly interstratified clays of compositions unknown in nature.

New synthetic randomly interstratified clays include:

all compositions wherein one component (of the two or more) is ammonium mica or paragonite, and all compositions having three or more clay components except for the following which are known in nature: illite-chlorite-smectite and i Ilite- smectite-vermicu lite.

Preferably, the suspension (i) and/or (ii) and/or (iii) and/or the mixed suspension is ultrasonically vibrated, preferably for 1-2 minutes. Preferably, the clay concentration in the suspension (i) and/or (ii) and/or (iii) is from 0.2 to 10 g/l, more preferably from 0.2 to 5 g/l; synthetic hectorite is one clay stable in suspension at the higher concentrations.

Preferably, the mixed suspension at step (iii) has, or is adjusted to have, a total clay concentration of from 0.2 to 10 g/l, more preferably from 0.2 to 1 g/l.

The steps (i) and (ii) of saturating the clays are intended to involve disaggregation of the clay materials to completely dispersed individual free particles (the 'elementary' or 'fundamental' particles of the clay) in colloidal suspensions. In this form, with no large incompletely dispersed particles, the clays in suspension can be mixed to form colloidal products and the mixed suspensions can be dried to form randomly interstratified aggregate products of different layer 2 GB2154998A 2 types in varying proportions.

A 'fundamental' particle is defined as an individual or free particle which yields a single crystal pattern by electron diffraction.

An 'elementary' particle is a specific type of fundamental particle, examples of which are 5 described below.

Three examples of clay materials which can be completely dispersed to elementary particles are:- (1) smectite (100% expandable layers), corresponding to single silicate (2: 1) layers, the particles being 1 OA thick; (2) rectorite (a regularly interstratified mica-smectite (50% expandable layers)), corresponding 10 to two silicate (2: 1) layers co-ordinated by a single plane of cations (i.e. Na +, N H +, or as in this case K+), the particles being 20A thick; and 4 (3) corrensite (a regularly interstratified chlorite-smectite, (50% expandable layers)) corresponding to two silicate (2: 1) layers co- ordinated by a single brucitic sheet, the particles being 24A thick. The 2:1 silicate layer is composed of 2 tetrahedral sheets and 1 octahedral sheet.

These particle thicknesses are determined by detailed transmission electron microscopy.

Smectite and vermiculite clays as well as clays with interstratification of illite, chlorite, kaolinite, ammonium-mica, paragonite or biotite layers with smectite and/or vermiculite layers may be used. Any mixture of the two or more of these clays, in any proportions, may be used in this invention. The composition of the product may thus be selected at will within the possibilities of these mixtures. An elementary product is randomly interstratified mica:smectite containing from 50 to 100% expandable layers.

The saturation may for example be accomplished by washing with 1 -3M solutions of NaCl or LiCl. After saturation the excess ions can be removed by centrifugation, the solution being decanted and the clay resuspended with distilled or deionated water, but more preferably, to 25 ensure quantitative retention of the dispersed material, the suspension containing the excess alkali metal ions is dialysed against distilled or deionised water. Most preferably of all, the saturation of the clay is achieved by using an alkali-metal-loaded cation exchange resin, whereby the step of removing excess alklai metal ions is avoided entirely.

Any suspended particles exceeding a 10-7 m equivalent spherical diameter may be removed 30 from the completely dispersed particles by centrifugation. X-ray diffraction of the resulting sediment confirms that the clays are completely interstratified. Mixed suspensions made as above of smectite with rectorite, and smectite with corrensite, yield X- ray diffraction patterns indentical to randomly interstratified illite-smectite and randomly interstratified chlorite-smectite respectively. The proportion of the layer types is determined by the relative amounts of the suspended components used to make the mixed suspension. Air drying of the mixed suspension on to a flat surface yields an aggregate product in the form of a film. Formation of the aggregate product may also be accomplished by freeze drying or spray drying. Sedimentation of the product from the suspensions may also be accomplished by adding a flocculating agent.

The invention will now be described by way of example.

EXAMPLES 1-4

Aqueuous suspensions were prepared of the smaller then 10-7M fraction of Nal-saturated smectite (Wyoming bentonite, Wards montmorillonite 25, John C. Lane tract, Upton, Wyoming, USA) and smaller than 10-7 m Na±saturated K-rectorite (bentonite, Lab number M13235, Canon 45 City, Colorado, USA, a regularly interstratified illite-smectite, with 50% expandable layers). The concentrations of the smectite and rectorite in the suspensions were 3.2 and 1.1 g/I respectively. The suspensions were mixed in solids weight ratios of the smectite to the rectorite of 1:1, 1:2, 1:4 and 1:8 (Examples 1, 2, 3 and 4). The mixed suspensions were dried on to glass slides, ethylene glycol solvated and analysed by X-ray diffraction. The diffraction maxima 50 are identical to naturally occurring randomly interstratified illite-smectite with 90-50% smectite layers. In the table, S is smectite, I is illite, and 001, 002, 003, 004 and 005 are the crystallographic planes.

3 GB2154998A 3 Interplanar spacings (in AJ as determined by Percent Ratio by weight X-ray diffraction maxima: expandable Example smectite:rectorite experimental (theoretical) layers S00211001 S00311002 1 1:1 8.60(8.59) 5.60(5.60) 90 2 1:2 8.86(8.81) 5.54(5.53) 70 10 3 1:4 9.01(9.03) 5.42(5.45) 55 4 1:8 9.09(9.14) 5.39(5.41) 50 EXAMPLES 5-7

Aqueous suspensions were prepared of the smaller than 10-7M fraction of Li±saturated smectite (saponite from Ballarat, California, USA) and the smaller than 10-7M fraction of Li-1- saturated corrensite (vein filling in dolerite from Hillhouse Quarry, Ayrshire, Scotland). The concentrations of the smectite and corrensite in suspension were both 0.4 g/l. The suspensions were mixed in weight ratios of the smectite to the corrensite of 2:1, 1:1 and 1:2 (Examples 5, 6 20 and 7). The mixed suspensions were subjected to 2 minutes' ultrasonic bath treatment.

Sedimental aggregates of the mixed suspensions were prepared on glass slides, ethylene glycol solvated and analysed by X-ray diffraction. The diffraction maxima are identical to randomly interstratified chlorite-smectite with 80-60% smectite layers. (The abbrevaitions are as before. S is smectite and C is chlorite.) Interplimar spacings (inA) as determined by Percent Ratio by weight X-ray diffraction maxima: expandable 30 Example smectite:rectorite experimental (theoretical) layers S0021C002 S0051C004 2:1 8.29(8.27) 3.39(3.41) 80 6 1-1 8.16(8.12) 3.42(3.42) 70 35 7 1:2 7.93(7.97) 3.44(3.44) 60 EXAMPLES 8-9

Aqueous suspensions of the rectorite and corrensite (previously described) were mixed in ratios by weight rectorite to corrensite 1A, 3A. Sedimented aggregates of the mixed suspensions were formed on glass slides, ethylene glycol solvated and analysed by X-ray diffraction. The maxima are identical to randomly interstratified smectite-illite-chlorite. (Abbreviations as before; S = smectite, 1 = illite, C = chlorite.) Interplanar spacings (in A) as determined by Percent Ratio by weight X-ray diffraction maxima: expandable Example rectorite:corrensite experimental (theoretical) S:l:C 50 S005110031C004 8 1:1 3.43(3.44) 40:20:40 9 3:1 3.39(3.36) 40:40:20 EXAMPLE 10

Aqueous suspensions of Nal-saturated smectite (Wyoming bentonite) and Krectorite (both previously described) were mixed in a ratio by weight of smectite to rectorite 1:2. The concentration of total clay in the mixed suspension was diluted with distilled water to 1 g/1. The 60 mixed suspension was subjected to ultrasonic bath treatment for 2 minutes. A sedimented aggregate was prepared on to a glass slide, ethylene glycol solvated and analysed by X- ray diffraction. The diffraction maxima are identical to a randomly interstratified illite-smectite, 75% smectite layers. (Abbreviations as before.) 4 GB2154998A 4 Interplanar spacings (in A) as determined by Percent Ratio by weight X-ray diffraction maxima: expandable Example smectite:rectorite experimental (theoretical) layers 5 1:2 S00211001 S00311002 8.75(8.75) 5.55(5.55) 75 In further experiments (not described in detail) a suspension of Lil- saturated Wyoming bentonite and corrensite and a suspension Nal-saturated Wyoming bentonite and corrensite yielded comparable results.

EXAMPLES 11-15 Aqueous suspensions were prepared of:

(i) the smaller than 10 - Irn fraction of Li + -saturated smectites (Wyoming bentonite, previously described) at 4.6 g/l; (ii) synthetic hectorite (a smectite prepared as described in Neumann, B. S., 1965, Rheol, Acta Vol. 4, page 250 and British Patent 1054111, obtained from Laporte Industries under the trade 20 name Laponite) at 10 g/l; and (iii) the smaller than 10-7 m Na ±saturated naturally occurring randomly interstratified kaolinite-smectite (75% kaolinite layers (i.e. 25% expandable layers), from Tepakan, Campeche, Mexico) at 5.8 g/l.

Suspensions of (i) and (iii) were mixed in solids weight ratios of 4:1 and 2:1 (Examples 11 25 and 12). Suspensions of (ii) and (iii) were mixed in solids weight ratios of 1: 1, 1:2 and 1:4 (Examples 13, 14 and 15). The five mixed suspensions were each subjected to 1 minutes' ultrasonic bath treatment. Sedimented aggregates of the mixed suspensions were prepared on glass slides, ethylene glycol solvated and analysed by X-ray diffraction. The diffraction maxima are identical to randomly interstratified kaolin ite-smectite with 95-40% smectite layers. (The 30 abbreviations are as before. S is smectite and K is kaolinite).

Interplanar spacings Ratio by (in A) as determined by Percent 35 weight smectite: X-ray diffraction maxima: expandable Example kaolinite-smectite experimental (theoretical) layers S0051K002 11 4:1 3.386(3.385) 95 40 12 2:1 3.390(3.390) 85 S0021K001 13 1:1 8.36(8.36) 75 14 1:2 8.09(8.13) 50 45 1:4 7.97(8.01) 40 EXAMPLES 16-18 Aqueous suspensions were prepared of the smaller than 10 - 'm fraction of Li ±saturated 50 smectite (Wyoming bentonite, previously described) and of Nal-saturated naturally occurring regularly interstratified illite-smectite (70% illite layers) (laboratory number MB91 2 from Los Piedras, Colorado, USA). The concentration of the interstratified illite- smectite was 2.7 9/1. The suspensions were mixed in ratios by weight of smectite to interstratified illite-smectite of 1 A, 1:2 and 1:3 (Examples 16, 17 and 18). The mixed suspensions were treated and analysed in 55 the same manner as those of Example 11 -15. The diffraction maxima are identical to randomly interstratified illite-smectite with 90-60% smectite layers. (The abbreviations are as before.) GB 2 154 998A 5 Interplanar spacings Ratio by (in A) as determined by Percent weight illite X-ray diffraction maxima: expandable Example illite-smectite experimental (theoretical) layers S00211001 S00311002 16 1:1 8.60(8.59) 5.61(5.60) 90 17 1.2 8.86(8.81) 5.54(5.53) 70 10 18 1.3 9.01(8.90) 5.51(5.50) 60 EXAMPLES 19-21 Aqueous suspensions were prepared of the smaller than 10-7M fraction of Lil-saturated 15 Wyoming bentonite (previously described) and of Na±saturated synthetic interstratified ammon ium-mica-smectite (60% ammonium-mica layers) (made as described in US Patent 3252757).

The concentration of the interstratified ammonium-mica-smectite was 5.7 9/1. The suspensions were mixed in weight ratios of the smectite to the interstratified ammonium mica-smectite of 1A, 1:2 and 1:3 (Examples 19, 20 and 21). The mixed suspensions were treated and analysed 20 in the same manner as those of Examples 11 - 15. The diffraction maxima are identical to randomly interstratified ammonium-mica-smectite, 90-70% smectite layers. (The abbreviations are as before. M is ammonium-mica.) Interplanar spacings Ratio by weight (in A) as determined by Percent smectite:ammonium- X-ray diffraction maxima: expandable Example mica-smectite experimental (theoretical) layers S0031M002 19 1:1 5.59(5.60) 90 1:2 5.57(5.57) 80 21 1:3 5.53(5.53) 70 EXAMPLE 22

Aqueous suspensions were prepared of the Li ±saturated smaller than 10-7 fraction of hydrobiotite (regularly interstratified biotite-vermiculite, 25% biotite layers) and of vermiculite, both of which had undergone treatment with large organic cations to cause gross expansion between the 2:1 silicate layers (Walker, G.F., 'Science' Vol. 156, pp. 385-387 (1967) and British Patent 10 16 385). The concentrations of hydrobiotite and vermiculite in the suspensions were 2.25 and 0.1 g/I respectively. The suspensions were mixed in a weight ratio of the vermiculite to hydrobiotite of 1:2. The mixed suspension was subjected to 1 minutes' ultrasonic bath treatment. Because X-ray identification of vermiculite is routinely based on its interplanar 45 spacing in the Mg2 I -saturated form (14.34 the clay materials in the mixed suspension were Mg2 + -saturated. A sedimented aggregate of the Mg2 + -saturated mixed suspension was prepared onto a glass slide and analysed by X-ray diffraction. The diffraction maxima are identical to randomly interstratified biotite-vermiculite with 90% vermiculite layers. (Abbreviations are as before. B is biotite, V is vermiculite.) Interplanar spacings Ratio by weight (in A) as determined by Percent vermiculite X-ray diffraction maxima: expandable 55 Example hydrobiotite experimental (theoretical) layers VOO 1 IBOO 1 V0041BOO3 22 1:2 14.2(14.2) 3,57(3.57) 90 60 EXAMPLE 23

This Example demonstrates that dispersed micro-crystalline and amorphous material can be combined with completely dispersed clay particles. Aqueous suspensions were prepared of:

(i) the smaller than 10-7M fraction of Li ---saturated smectite (being synthetic hectorite 65 (previously described)) and 6 GB2154998A 6 (ii) proto-imogolite (Farmer, V.C. and Fraser, A.R., Proceedings of the Sixth International Clay Conference (pp 547-553), ed. M.M. Mortland and V. C. Farmer, Elsevier, Amsterdam, 1979, and Farmer, V.C., British Patents 1574954 and 2025384).

The suspensions were mixed in a weight ratio of the smectite to the protoimogolite of 1:1. The mixed suspension was subjected to 1 minutes' ultrasonic bath treatment. A sedimented aggregate of the mixed suspension was prepared onto a glass slide and heated to 300'C for 2 hours; a sedimented aggregate of the synthetic hectorite alone was heated to 300'C for 2 hours for comparison. Both were analysed by X-ray diffraction. The X-ray diffraction maxima show the sedimented aggregate made from the mixed suspension to have a random range of spacings from 10.5A up to an undetermined upper limit (greater than 34A), whereas the smectite layers 10 of the sedimented aggregate made from the suspension of synthetic hectorite alone collapsed to a more uniform spacing of 9.78A. The results demonstrate that the dispersed amorphous protoimogolite particles have become randomly interposed between the clay smectite layers.

EXAMPLE 24

Aqueous suspensions were prepared of the Na±saturated smaller than 1 01m fractions of rectorite from Baluchistan, Pakistan (regularly interstratified paragonite-smectite, 50% paragon ite layers) and of Wyoming bentonite (previously described), the concentration of the rectorite suspension being 2.4 g/l. The mixed suspension was subjected to 1 minutes' ultrasonic bath treatment. A sedimented aggregate of the mixed suspension was prepared onto a glass slide, 20 ethylene glycol solvated and analysed by X-ray diffraction. The diffraction maxima are identical to a randomly interstratified paragonite-smectite with 90% smectite layers. (The abbreviations are as before. P = paragonite and S = smectite.) Ratio by weight Example rectorite:smectite Interplanar spacings (in A) as determined by Percent X-ray diffraction maxima: expandable experimental (theoretical) layers 24 1:1 S0021P001 S0031P002 8.59(8.60) 5.64(5.59) 90 NOTE: All theoretical X-ray diffraction values are taken from Reynolds, R. C., Interstratified 35 Clay Minerals, Chapter 4 (pp 249-303) in Crystal Structures of Clay Minerals and their X-ray Identification, edited by G. Brindley and G. Brown, Monograph 5, Mineralogical Society, London, 1980. Although the invention has been demonstrated primarily for conventional interstratified clays, the invention is applicable to any two or more of the dispersed clay minerals.

Claims

1. A method of synethesising a randomly interstratified clay, comprising:

(i) saturating (replacing all the exchangeable cations of) a first clay which is either fully expandable or contains an expandable component, with alkali metal ions, removing any excess 45 alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 10-1m equivalent spherical diameter, (ii) separately or together saturating a second clay which is either fully expandable or contains an expandable component, with alkali metal ions, removing any excess alkali metal ions, and forming the saturated clay into a suspension containing no suspended particles exceeding 50 10-1m equivalent spherical diameter, (iii) forming a mixed suspension from the suspensions from (i) and (ii), and (iv) sedimenting the mixed suspension, the sediment being the synthetic randomly interstrati fied clay.

2. The method of Claim 1, wherein the alkali metal ions with which the first clay is saturated 55 are selected from Nal and Li+.

3. The method of Claim 1 or 2, wherein the alkali metal ions with which the second clay is saturated are selected from Na+ and Li+.

4. The method of any preceding claim, further comprising drying the sedimented mixed suspension.

5. The method of any preceding claim, wherein the sedimentation of the product from the mixed suspension is accomplished by adding a flocculating agent.

6. The method of any preceding claim, further comprising saturating the sediment (which may be dried) with a cation.

7. The method of any preceding claim, further comprising saturating at least a third like clay 65 7 GB 2 154 998A 7 and forming the third and any further clay into a suspension in like manner as the first and second clays, and forming a mixed suspension from all the suspensions.

8. The method of any preceding claim, wherein at least one of said suspensions is ultrasonically vibrated.

9. The method of Claim 1, wherein the clay concentration in at least one of said suspensions 5 before mixing is from 0.2 to 10 9/1.

10. The method of Claim 9, wherein the clay concentration is at least one of said suspensions before mixing is from 0.2 to 5 g/1.

11. The method of any preceding claim, wherein the mixed suspension has, after adjust- ment if necessary, a total clay concentration of from 0.2 to 10 g/1.

12. The method of Claim 11, wherein the mixed suspension has, after adjustment if necessary, a total clay concentration of from 0.2 to 1 g/1.

13. The method of any preceding claim, wherein the component clays include at least one of smectite, illite, paragonite, chlorite, kaolinite, ammonium-mica, biotite and vermiculite.

14. The method of Claim 1, substantially as hereinbefore described with reference to any 15 one of Examples 1 to 24.

15. A randomly interstratified clay made by the method of any preceding claim.

16. Synthetic radomly interstratified clay.

17. The randomly interstratified clay of Claim 15 or 16, containing at least one of ammonium-saturated mica and paragonite.

18. The randomly interstratified clay of Claim 15, 16 or 17, containing at least three clay components.

19. An intermediate usable in the method according to any of Claims 1 to 14, being a suspension containing no suspended particles exceeding 10-7 m equivalent spherical diameter, and made by saturating a clay with alkali metal ions and removing any excess alkali metal ions. 25

20. The intermediate of Claim 19, made with the feature(s) recited in any of Claims 2, 8, 9, 10 or 13.

Printed in the United Kingdom for Her Majesty's Stationery Office, Dd 8818935. 1985, 4235 Published at The Patent Office. 25 Southampton Buildings. London. WC2A 'I AY, from which copies may be obtained.